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42D09SE8295 42D09SE00l4 fil MUSSY LAKE010
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REPORTon
CITADEL MINES LIMITEDMOLYBDENUM-NICKEL PROPERTYPlayter Harbour
Area, Lake Superior
Sault Ste. Marie Mining DivisionDistrict of Thunder Bay,
Ontario
SSM-
Toronto, Ontario
r. O, -P,
OJUN 6 1969
RESIDENT GEOLOGISTSAULT STE. MARIE
December 11, 1968
NOT TO BE REMOVED FROM
THE OFFICE OF THE RESIDENT
GEOLOGIST, ONT. DEPT. OF MINES
SAULT STE. MARIE. ONT.
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12D09SE829S 42D09SE00 MSI MUSS "LAKE"
INDEX-
SUMMARY
INTRODUCTION
PROPERTY
ACCESS
POWER
HISTORY
GENERAL GEOLOGY
SHOWINGS
AEROMAGNETICS
SAMPLING
SUMMARY AND CONCLUSIONS
RECOMMENDATIONS
COST
ACKNOWLEDGEMENTS
CERTIFICATE
MAPS
1
2
2
2
3
3
4
5
6
7
8
9
10
12
13
SSM-1383
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SUMMARY
Citadel Mines Limited has acquired an option to
purchase a block of 80 contiguous unpatented mining claims
situated
in the Playter Harbour Area, on the north shore of Lake
Superior.
The claims cover a 5j mile length of a belt of
greenstone characterized by deep east-west valleys occupying
fault zones and a relatively high band of magnetics.
A molybdenite-bearing quartz body was found in
one of these valleys in the 1930's and four trenches put
down.
During this past summer and fall the deposit has twice been
sampled with encouraging results,
A program cFtimated to cost S32, 500 has been
recommended:
1. To sample and delimit the known molybdenite-
bearing quartz bodies using BX sized diamond drill core.
2. In conjunction with this that magnetic and
electromagnetic surveys be conducted over the valley bottom
for at least one mile.
3. That anomalies found by the geophysical
surveys bc investigated by diamond drilling.
1 *.''.t,
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INTRODUCTION
Citadel Mines Limited has acquired an option to
purchase a block of 80 claims, covering an old molybdenite
and
a zinc-nickel-copper prospect, located in the Playter Harbour
Area
of Lake Superior.
PROPERTY
The property on which Citadel Mines Limited holds
an option consists of 80 contiguous unpatented mining claims
located
in the Sault Ste. Marie Mining Division of Ontario and shown on
the
Ontario Department of Mines Plan No. M-29.
These claims were recorded on July 12, 1968 and
have been tagged. Their numbers follow:
S.S. M. 103273 to S.S. M. 103284 incl. 12 claims
S. S. M. 103303 to S. S. M. 103370 incl. 68 claims
Total 80 claims
ACCESS
The group lies east of Playter Harbour on the
north side of Lake Superior, about six miles south of Heron
Bay,
Ontario. Playter Harbour is'accessible in summer by boat
from
the mouth of the Pic River or float planes based at White
River
44 miles distant. A trail, about 2 miles in length, leads
from
the beach at the east end of Playter Harbour to the
molybdenite
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5
showing. Across the mouth of the Pic River, where the motor
road ends, a trail about 5 miles in length leads to the same
showing.
This trail with a little work could be made into a tractor road
and
provide an all season route to the property. Access, at
present,
to the copper-nickel showing is most easily gained by flying
from White River.
POWER
The new transmission line for the Inter-Provincial
Power Grid System passes over the copper-nickel showing.
Power
is expected to be turned on in late 1969 or early 1970.
HISTORY
The molybdenite showing was first staked for gold
around 1930. No gold or silver was found and with no interest
in
molybdenite, work ceased.
In late 1930's the showings were reportedly
.investigated by Consolidated Mining and Smelting Co. for
molybdenum. Rock trenches were put down and bulk samples
taken, but the results of this work are not available.
The clainvgroup containing the molybdenite showing
was subject of a report by Mr. D. M. Arnott, P. Eng. dated
17th
September, 1965. Mr. Arnott spent 5 days on the property
tying
SSM-1383
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p
in and mapping the showing and examining the geology of the
claim group.
Kennco Explorations Canada sampled two of the
rock trenches put down on the quartz body in July 1968.
Later on September 21, 1968, Dr. T. C. James
of W. G. Wahl Limited, sampled the four trenches.
The copper-nickel showing was dibcovered late
in the fall of 1965 and was partly opened up by two rock
trenches,
20 f co t ?part.
GENERAL GEOLOGY
From geological maps Nos. 40-d and 41-j of the
Ontario Department of Mines the claim group is shown to be
underlain by undifferentiated basic volcanics of Keewatin
age.
Intruding these arc Algoman feldspar porphyry dikes. All the
above are cut by late diabase di kcs
The predominant rock typcsobservod on the ground
were basic lavas that have been altered to hornblende schists.
In
and around the vicinity of the copper-nickel showing graphitic
tuffs
were observed.
Several east-west ridges cross the property and
are separated by deep narrow valleys. Wherever rock has been
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seen in the floor of these valleys it is strongly sheared and
the
evidence is that they arc caused by regional faulting. This
feature stands out on the aerial photos, which also show a
number of oblique lineaments crossing the cast-west valleys.
SHOWINGS
1. The molybdenite showing is presently of the most
economic interest.
The showing occurs on the bottom of one of the
deep cast-weat trending valleys, in the southeast corner of
claim
S. S. M. 103306. It consists of an east-west striking quartz
vein
which has been c-xposed over a length of 133 feet before1
disappearing under overburden at either end. Coarse grained
amphibolite forms the north wall, while that on the south is
biotite schist. Both walls are highly sheared in the
vicinity
of the vein. At no place are the contacts exposed, though
one
trench has been sampled over 40 feet. A 10 foot creek
prevented
further trenching to the south. The dip of the quartz vein
appears
to be steeply to the south, while the schistose wall rock
apparently
Hips steeply to the north.
The strong fault zone in which the showing
occurs is topographically defined for several miles. About
2500 feet to the east an outcrop of quartz is exposed in the
bed
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of the creek. To the west, 1500 feet away, another outcrop
of
quartz occurs.
Molybdenite is present in significant amounts
and is directly proportional to the degree of fracturing. It
ranges from 1/4" thick in strong fractures to disseminated
molybdenite associated with incipient fractures in quartz
that
otherwise appear massive. The fractures tend to be parallel
to the strike of the vein,
2. The copper-nickel occurrence lies near the
cast boundary of claim S. S. M. 103322 in another of those
narrow east-west valleys. The valley is covered with deep
overburden and the trenching only exposed 16 feet of the
north
side of the mineralized zone, which judging from the
topography,
could bc 60 feet wide.
The two trenches exposed a highly sheared
graphitic tuff well mineralized with pyrite, pyrrhotite and
minor
chalcopyrite. Only low copper and nickel values were
obtained
from here, but much of the zone remains to be tested.
AEROMAGNETICS
The government aeromagnetic map entitled "Heron
Day" and numbered 2156G shows a strong, persistent cast-west
j
SSM-1383
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anomaly running the length of the claim group and extending
beyond it for around l 1/2 miles. Its width is approximately
that of the property and it stands out above a broad plain
of
readings 1000 to 1500 gammas lower.
SAMPLING
No records are available for the original bulk
sampling carried out by Consolidated Mining and Smelting
Company in the 1930's, on the molybdenite showing.
On July 15th of this year Kennco Exploration
Canada Limited made an examination of the molybdenite
showing and obtained;
Location Type of Sampling Length
0. 21ty MoS
0. 567c MoS,
Average 40. O 1
W. branch Main Tr. representative grab 35. O 1
On September 21, 1968 Dr. T. C. James took bulk and
chip samples from the four trenches as described in the report
by
B. M. Arnott. There were only 3 samples taken and it i t s
urmised
S S"', i r- l o
F
E. branch Main Tr. representative grabN to S
2. 0'6. 0 7. 0
25. 0
2. 640. 09 0. 100. 08
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that sampling from the two shorter trenches has been
combined
in one sample.
This sampling resulted in:
Bulk Samples Chip Samples
No.
316 318 320
Wt.
600 690 690
Length
31' 37' 49'
ft MoS2
0. 07 0. 11 0. 17
VrPbS
0. 057 0. 068 0. 034
No.
317 318 321
Length
31'37' 49.
7r MoS2
0. 29 0. 16 0. 20
Average, weighted for Average, weightedLength 0. 12"ftMoS2 for
length 0.
The chip samples were taken from each fragment constituting
the bulk samples.
Mr. A mott 1 s sampling of the 16 feet of the copper-nickel-
zinc showing exposed in the trenching ran 0. 95^c Zn, 0. 06^r Cu
and
0. 057r Ni. This could represent only the fringes of the zone
as
from the topography the zone is thought to have a width of
around
60 feet.
SUMMARY AND CONCLUSIONS
The molybdenite showing is associated with a large
quartz vein occurring in a strong fault zone that can be
traced
for miles. The valley of the fault zone is mostly
overburdened
but three exposures of quartz occur over a length of 4000
feet.
SSM-1383
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At the one exposure opened up molybdenite occurs
over .1 width of at least 40 feet. The amount of mineralization
is
directly proportional to the degree of fracturing, which
runs
parallel to the vein.
The sampling results from the one exposure opened
up are definitely encouraging.
The exploration possibilities of finding other fractured
molybdenite-bearing quartz veins are deemed excellent. Some
of
these a re:
(a) Along the fault zone in which the known showings occur.
(b) The locale of the conjunction of the east-west shearing
with oblique lineaments.
(c) Other deep east-west valleys, which may represent
other fault zones and contain other molybdenite-
bearing quartz veins.
While low, the copper-nickel-zinc values are of
interest as it is likely that only the fringe of the mineralized
zone
is exposed and the geological environment is good.
RECOMMENDATIONS
For the present that all exploration be directed
toward finding an economic molybdenum deposit. To this end
that
the following be carried out.
S S.M -
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L That the presently known quartz bodies be sampled
by, 50 foot spaced, BX sized diamond drill holes.
2. That in conjunction with this, electromagnetic and
magnetic surveys be carried over the valley floor
for at least one mile. The spacing of the lines to
be at 50 foot intervals to start with and later the
spacing to be dictated by the experience gained.
The quartz bodies should show as magnetic lows
and with the fracturing running parallel the vein
the larger molybdenite fractures should give an
electromagnetic response.
3. That a little step-out drilling be done to test
anomalies picked up in the survey.
4. That further exploration await the results of this
initial phase.-
COST
To carry out this initial phase of exploration the
cost is estimated to be:
1. Diamond drilling - 3000 ft. of BX core@ $S. 5 0/ft. $l6, 500.
00
2. 150 core trays @ S2. 00 per tray 300. 00
3. Snowmobile and sled 1,200.00
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4. Tent and frame 14' x 18', plywood floors and ten test walls
or completely ten touted (roof plywood and ten test), Coleman oil
stove, lantern, bunks, :; mattresses, shovels, pails, hammer etc. |
l, 400. 00 jt
IS. Electromagnetic and magnetic surveys 1,500.00
"** 6. . Bulldozing out trail to make tractorroad - 5 miles 2,
000. 00
7. Supervision, engineering, assaying,
transportation, core splitter, sample bags, gas and oil, meals,
contingencies 9, 600. 00
tj
Total 3 32,500. 00
Respectfully submitted,
G. E. Moody, B. Se. , P. Eng.
Toronto, Ontario
December 11, 1968
SSM-1383
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PGHD CONSULTANTS LIMITED !
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ACKNOWLEDGEMENTS
Ontario Department of Mines - Vol. XL, Part 2 , 1 931,
entitled"Geology of the Heron Bay Area, Districtof Thunder Bay"
- Map 41-J - "Heron Bay -White Lake Area"
Reports by B. M. Arnott, P. Eng. dated September 17, 1935 and
February 9, 1966.
Personal communique Kennco Explorations Canada Ltd.
Geophysical Paper - Heron Bay - Map 2156G.
Aerial Photos of the property.
Report by Dr. T. C. James dated September 27, 1968.
C--'
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-- ""CERTIFICATE \
t.i
l, George E. Moody, of the Town of Beaverton, in ij
the Province of Ontario, hereby certify: \
1 1 1 -1 1
l ll 3
1. That I am a consulting mining engineer with offices situated
at 541 Osborne Street, Beaverton, Ontario and at Suite 209, 185 Bay
Street, Toronto, Ontario.
2. That I am a graduate in mining engineering from the
University of Alberta (1931) and have practised my profession
continuously since my graduation.
3. That I am a member of the Corporation of Engineers of the
Province of Quebec and a Fellow of the Geological Association of
Canada.
4. That l have no direct or indirect interest, nor do l expect
to receive any direct or indirect interest in the property
described herein. I do not own beneficially, directly or indirectly
any shares in Citadel Mines Limited nor shares in any affiliate of
that Company.
5. That my report on the Playter Harbour Areaproperty, situated
in the Sault Ste. Marie Mining Division and shown on Plan M-29 of
the Ontario Department of Mines, is based on:
(a) Ontario Government Geological publications and maps.
(b) Reports on the property by B. M. Arnott, P. Eng. dated
September 17, 1965 and February 9, 1966.
(c) Report by Dr. T., C. James dated September 27, 1968.
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(d) Personal communique Kennco Explorations Canada Ltd.
(c) Data in the Company's files.
DATED at Toronto this lith day of December, 1968.
G. E. Moody, B. Se. P. En g.
SSM- 1383
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42D09SE829S 42D09SE0014BI MUSSY LAKE020
XL DIRECTOR l '-.'.'-fi UAt^,.-*
SUMMARY REPORT ON CITADEL MINES LIMITED
MOLYBDENUM-NICKEL PROPERTY Playter Harbour Area, Lake Superior
Sault Ste. Marie Mining Division District of Thunder Bay,
Ontario
Toronto, OntarioDecember 11, 1968
-
Summary Report
The following summary is provided by G.E. Moody, B.Sc.,P.Eng
whose full report is available in the Public Files of the
Ontario Securities Commission.
Citadel Mines Limited has acquired an option to purchase a
block
of 80 contiguous unpatented mining claims, situated in the
Playter Harbour Area of the Sault Ste, Mining Division of
Ontario.
The property is presently accessible by a trail from the
mouth
of the Pic River, or by boat from there to Playter Harbour,
and thence by a 2 mile trail to the molybdenite showing.
Planes, based at White River can land at Playterjs Harbour.
The claims cover a 5^ mile length of a belt of greenstone
characterized by deep east-west valleys occupying fault
zones
and a relatively high east-west band of magnetics.
In one of these valleys a molybdenite-bearing quartz body
was found. Consolidated Mining and Smelting put down four
trenches on it in the late 1930's and bulked sampled the
deposit, the results of which are not available.
SSM-138 S
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In 1968 two companies ' iinpled the showing and obtained
encouraging
result^ over widths up to 40 feet. The valley is heavily
overburdened and the full width and length of the quartz body
is
not known. Untested quartz exposures lie respectively 2,500
feet
to the east and 1,500 feet to the v;ost,
In view of the above it is recommended that sampling and
exploration of this showing be carried out using BX sized
drill
rods. That an electromagnetic and magnetic survey be carried
out along this valley bottom to help in delineating the
known
quartz occurrences and to help pick up other bodies. Any
anomalies picked up are to be tested by diamond drilling.
Further exploration will be contingent on results gained
during
this initial program.
GHD Consultants Limited,
G.E. Moody, B.Sc.,P. Eng.
Toronto, Ontario December 11, 1968.
SSM- 1033
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t20e9SE8295 42D09SE00HB1 MUSSY LAKE
CLAIM
S. S.
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103273103274103275103278103279103280103281103282103283103284
1. 103303103304ion 0 5umo(.103307103308103 3
(H103410103311103312103313103314103315103316103317103318103319103320103321i..
33241033?'-.
103326103327101328H'^329
, . 0103331103332
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CLAIMS A F
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CITADEL MINES
DAYS
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LIMITED j
fCLAIM
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10333310333410333510333610333710333810333"103340103341103342(0334310334410334-10334610334710334
S10334')10335010335110335210335310335410335510335610335710335810335"103360103361103362103363103
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RESIC-NAL DIRECTOR
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TO EACH OTHER.
-
##ONTARIO
THE MINING ACT REPORT OF.WORK
A ••eerete fern l* required fer eech tye* ef w** te V*
feeerdee.
To the Recorder ef . Di vi* Ion
C 2??tii tf •••••fTfrivt ..*M*ie ef Recorded Holder. P t, M
iner'(Licence
.. .... ..TMV. rf^ft^ttk^'. G^X-.' Sfe * ** 'XJZZ^ftfrs
Gtrfc,".................................^..^.^^^......^.. .....
...... . .. ...................^
de hereby report the performonce of
................./?.5?................. doy* of ,
,a}.J.K.(jS.R.(f),4,K'.frKj2type of work
not before report d to be applied on the following contlfuout
clolm*
Claim No. Day* Claim No. Day* Claim No. Day*
A O
Ail the work wo* performed on Mining Cloim (i)
....^..^/..../.ff..^.^^/^.:..............................................(In
the COM of geological ond/or geophyticol survey (s) where more than
18 claims are involved attach a schedule)
READ CAKtFULLY: THE FOLLOWING INFORMATION IS REQUIRED BY THE
MINING RECORDER.
Fer Manual Work, Stripping or Opening up of Mines, Sinking
Shafts or Other Actual Mining Operations - Names andoddresiM of the
men who performed the work ond the dates ond hours of their
employment,For Diamond ond other Core Drilling - Footage, No. ond
angle of hole* ond diameter of core. Name ond address ofowner or
operator of drill. Dates when drilling wan done. Sign*d core log
and sketch in duplicate.For Compre**ed Air or Other Power Driven or
Mechanical EquipmentType of drill or equipment. Names ond addresses
of men engaged in operating equipment ond the dates and hours
oftheir employment.For Power Stripping - Type of equipment. Name
ond oddrei* of ovner or operator. Amount expended. Date* on
whichwork wa* done. Proof of actual cost mutt be submitted within
30 day* of recording.With each of the above type t of work sketches
ore required to (how the location ond extent of the work in
relationte the nearest cieim poit. In the cose of diamond or other
core drilling the sketch *utt be submitted in duplicate.Fer
Geological ond 6eophy*lcel Survey - The now e i ond oddrette* of
men employed o* well os ditefi. ty***?*t iinstrument u*ed in the
case of geophysical survey. Reports and maps in duplicate must be
fill,within 60 days of recording.For Lend Survey - the name and
address of Ontario Land surveyor.
Tiie Mining Act Certificate Verifying Report of Work
L..^f..xv......3..6.-*......3.to.^.f/^^(Post Office Address)
'
Kor eby certify:
1. That l have o personal ond intimate knowledge of thu foctt
tet forth in the report of work annexed here to, having performed
the work or witnetted some during and/or after its completion.
2. That the annexed report it true.
..^#...,.^.......J9^' Sinature
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MARATHON
HIGHWAY 17
yERON BAY
ic R TVER
LAKE SUPERIOR
CLAIM GROUPI MAP SHOWING
LOCATION!- ACCESS ROUTESCITADEL MINES LTD
HERON BAY AREA. ONTARIO SCALE: 1.INCH - Z. MILES
l
PLAY HARB
-
MfDRO- ELECTRIC
POWER UN
MOHC^DENUU SHOW o,
NI-CU SHOWING
Late Diabase dyke
Algoman granite and gnel
Keewatin ba*ic volcanic*(some Algoman intrucives)
CITADEL MINES LTD-PROPERTY a
GEOLOGY MAP -
GtnFcONSULT AMICE i.T*
•CALK l INCH* 1/2 UU.C